FACT SHEET Tropical Cyclone Monica
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Known Impacts of Tropical Cyclones, East Coast, 1858 – 2008 by Mr Jeff Callaghan Retired Senior Severe Weather Forecaster, Bureau of Meteorology, Brisbane
ARCHIVE: Known Impacts of Tropical Cyclones, East Coast, 1858 – 2008 By Mr Jeff Callaghan Retired Senior Severe Weather Forecaster, Bureau of Meteorology, Brisbane The date of the cyclone refers to the day of landfall or the day of the major impact if it is not a cyclone making landfall from the Coral Sea. The first number after the date is the Southern Oscillation Index (SOI) for that month followed by the three month running mean of the SOI centred on that month. This is followed by information on the equatorial eastern Pacific sea surface temperatures where: W means a warm episode i.e. sea surface temperature (SST) was above normal; C means a cool episode and Av means average SST Date Impact January 1858 From the Sydney Morning Herald 26/2/1866: an article featuring a cruise inside the Barrier Reef describes an expedition’s stay at Green Island near Cairns. “The wind throughout our stay was principally from the south-east, but in January we had two or three hard blows from the N to NW with rain; one gale uprooted some of the trees and wrung the heads off others. The sea also rose one night very high, nearly covering the island, leaving but a small spot of about twenty feet square free of water.” Middle to late Feb A tropical cyclone (TC) brought damaging winds and seas to region between Rockhampton and 1863 Hervey Bay. Houses unroofed in several centres with many trees blown down. Ketch driven onto rocks near Rockhampton. Severe erosion along shores of Hervey Bay with 10 metres lost to sea along a 32 km stretch of the coast. -
6. Annual Review and Significant Events
6. Annual Review and Significant Events January-April: wet in the tropics and WA, very hot in central to eastern Australia For northern Australia, the tropical wet season (October 2005 – April 2006) was the fifth wettest on record, with an average of 674 mm falling over the period. The monsoon trough was somewhat late in arriving over the Top End (mid-January as opposed to the average of late December), but once it had become established, widespread heavy rain featured for the next four months, except over the NT and Queensland in February. One particularly noteworthy event occurred towards the end of January when an intense low (central pressure near 990 hPa) on the monsoon trough, drifted slowly westward across the central NT generating large quantities of rain. A two-day deluge of 482 mm fell at Supplejack in the Tanami Desert (NT), resulting in major flooding over the Victoria River catchment. A large part of the central NT had its wettest January on record. Widespread areas of above average rain in WA were mainly due to the passages of several decaying tropical cyclones, and to a lesser extent southward incursions of tropical moisture interacting with mid-latitude systems. Severe tropical cyclone Clare crossed the Pilbara coast on 9t h January and then moved on a southerly track across the western fringes of WA as a rain depression. Significant flooding occurred around Lake Grace where 226 mm of rain fell in a 24-hour period from 12 t h to 13 t h January. Tropical cyclone Emma crossed the Pilbara coast on 28 th February and moved on a southerly track; very heavy rain fell in the headwaters of the Murchison River on 1s t March causing this river’s highest flood on record. -
Summary of 2005/6 Australian-Region Tropical Storm Season and Verification of Authors’ Seasonal Forecasts
Summary of 2005/6 Australian-Region Tropical Storm Season and Verification of Authors’ Seasonal Forecasts Issued: 15th May 2006 by Professor Mark Saunders and Dr Adam Lea Benfield Hazard Research Centre, UCL (University College London), UK. Summary ¢¡¤£¦¥¨§¨§¨© £¨¨ £¨£¨ ¨£"!$#%¨&('(¨)¨'*+%,¨-'(.¨&/%¨01¨.%'23'(%546¨7+£¨ ¤£¨ ¨£8!$#%¨&('(¨9&*¨¤7:¨&(&*'( ;¨.%'23'*%54=<3 ¢¡¤'*>.¨¤%¨%?@'(%¡9%¡£A:B¨#A-,£C3'(¨#/!$#%¨&('(¨ %,¨-¤'*.¨&%¨0D£¨¨E@¡'(.¡F¨&(&3¡¤¨7F)£&(,@£¨ ¨£"¨.%'23'(%54¨<G ¢¡£" ¢HIJ%£,.'(&(£K-,¨)¤¨)'(&*'(%54 :B¨,£.¨%¦:L¨M%¡¤£¥¨§¨§¨© N £¨¨O¡,@£7P£Q¨.£&*&(£%$R¤'*&(&(ST-,£7'(.%'( :,¨0VUW 4X¥¨§¨§¨©+%¡¨% !K#%¨&('*¨ )¨'( ¨7 &(¨7¤:¨&*&('( Y¨.%'Z3'(%54Y[¨#&(7 )£\.&*¨£\%Y£¨ ¨£<X ¢¡¤£] ¢H¤I 7¤£%£0^'*¤'*%'*.¦:B¨,£.¨%A¡,@£76 ¨¨¨76R¤'*&(&_:B¨;)¤¨'(`¨.%'23'(%54a¨76:B¨¦&*¨¤7:¨&(&*'( M%,¨-'(.¨& %¨0b¤#0^)£_:,¨0bUc 4d¥¨§¨§¨©¨< egf3hejilk m3n(opqsr=t k iu1vKn(wyxOze{r|vK}$ok ~3wk it nZ¨u1m¨ilhwh~¨tNw@pFwy¨u[upiOk¨st(f3h¨¨¨ ^"3wyt(ilpq(n*p~3 ilh,¨n(k ~;t*ilk m3n(opqwtNk iyuwhpwk ~9p~3¦p8gpq(n(¨pt n(k ~k¨t(f3hniwhpwk ~3pqm¨ilk 3p3n(q*n(wyt n(oAp~3¦¨ht hiunZ~3n(wyt n*o k ilhopwyt w>k i?t(f3n(w>potNn 3nZt*¨¤egf3hwh$k ilhopwyt w{@hilh$n*wwy3hKuk ~¨t(f3qZ95ilk ut*f3h$ t(f¦Wp9¨¨¨ "tNk"t*f3h t(f@hohu[3hi8¨¨¨ p~3nZ~3oqZ3¨hKwhm3pilptNhTm¨ilh¨n(otNn(k ~3wsk i{~¨¨u3hilwsk¨¤t*ilk m3n(opqwyt k iuw~¨¨u[3hilw k¨¢wh¤hilh t(ilk m3n(opq¡oC3oq(k ~3hw"p~3¢t(f3h A£E¤¥z5@oo¨u3q(ptNh^£E3oq*k ~3h¦¤¡~3hi 3}snZ~3¨h§3egf3h[q*pt(tNhiKn(w ¨n ¤h~dk i¨t*f3h/"f3k¨q(h/"3wyt(ilpq*n(p~35ilh ¨n(k ~3 Features of the 2005/6 Australian-Region Season • The 2005/6 Australian-region tropical storm season featured 11 storms of which 7 made severe tropical cyclone strength (U.S. -
Polarimetric Radar Observations of the Persistently Asymmetric Structure of Tropical Cyclone Ingrid
616 MONTHLY WEATHER REVIEW VOLUME 136 Polarimetric Radar Observations of the Persistently Asymmetric Structure of Tropical Cyclone Ingrid PETER T. MAY,J.D.KEPERT, AND T. D. KEENAN Bureau of Meteorology Research Centre, Melbourne, Australia (Manuscript received 3 November 2006, in final form 3 May 2007) ABSTRACT Tropical Cyclone Ingrid had a distinctly asymmetric reflectivity structure with an offshore maximum as it passed parallel to and over an extended coastline near a polarimetric weather radar located near Darwin, northern Australia. For the first time in a tropical cyclone, polarimetric weather radar microphysical analyses are used to identify extensive graupel and rain–hail mixtures in the eyewall. The overall micro- physical structure was similar to that seen in some other asymmetric storms that have been sampled by research aircraft. Both environmental shear and the land–sea interface contributed significantly to the asymmetry, but their relative contributions were not determined. The storm also underwent very rapid changes in tangential wind speed as it moved over a narrow region of open ocean between a peninsula and the Tiwi Islands. The time scale for changes of 10 m sϪ1 was of the order of 1 h. There were also two distinct types of rainbands observed—large-scale principal bands with embedded deep convection and small-scale bands located within 50 km of the eyewall with shallow convective cells. 1. Introduction larimetric radar (Keenan et al. 1998). Ingrid was a long- lived storm that reached Australian category 5 intensity The structure and intensity of tropical cyclones (TCs) twice—initially before it crossed the North Queensland around landfall are a major topic of research because of coast, and then again as it reintensified over the Gulf of the potential impact on human populations and prop- Carpentaria, where the eye structure was quite sym- erty. -
KUNINJKU PEOPLE, BUFFALO, and CONSERVATION in ARNHEM LAND: ‘IT’S a CONTRADICTION THAT FRUSTRATES US’ Jon Altman
3 KUNINJKU PEOPLE, BUFFALO, AND CONSERVATION IN ARNHEM LAND: ‘IT’S A CONTRADICTION THAT FRUSTRATES US’ Jon Altman On Tuesday 20 May 2014 I was escorting two philanthropists to rock art galleries at Dukaladjarranj on the edge of the Arnhem Land escarpment. I was there in a corporate capacity, as a direc- tor of the Karrkad-Kanjdji Trust, seeking to raise funds to assist the Djelk and Warddeken Indigenous Protected Areas (IPAs) in their work tackling the conservation challenges of maintain- ing the environmental and cultural values of 20,000 square kilometres of western Arnhem Land. We were flying low in a Robinson R44 helicopter over the Tomkinson River flood plains – Bulkay – wetlands renowned for their biodiversity. The experienced pilot, nicknamed ‘Batman’, flew very low, pointing out to my guests herds of wild buffalo and their highly visible criss-cross tracks etched in the landscape. He remarked over the intercom: ‘This is supposed to be an IPA but those feral buffalo are trashing this country, they should be eliminated, shot out like up at Warddeken’. His remarks were hardly helpful to me, but he had a point that I could not easily challenge mid-air; buffalo damage in an iconic wetland within an IPA looked bad. Later I tried to explain to the guests in a quieter setting that this was precisely why the Djelk Rangers needed the extra philanthropic support that the Karrkad-Kanjdji Trust was seeking to raise. * * * 3093 Unstable Relations.indd 54 5/10/2016 5:40 PM Kuninjku People, Buffalo, and Conservation in Arnhem Land This opening vignette highlights a contradiction that I want to explore from a variety of perspectives in this chapter – abundant populations of environmentally destructive wild buffalo roam widely in an Indigenous Protected Area (IPA) declared for its natural and cultural values of global significance, according to International Union for the Conservation of Nature criteria. -
TROPICAL CYCLONE INFORMATION SERVICE Prepared by Coastal Services Unit, Environmental Sciences Division
TROPICAL CYCLONE INFORMATION SERVICE Prepared by Coastal Services Unit, Environmental Sciences Division Interim report on severe tropical cyclone Ingrid Issued April 2005. • Category 5 cyclone with wind gusts to 320 kilometres per hour near the centre. • Cyclone crossed the Queensland east coast as category 4, 57km south east of Lockhart River. • Estimated peak water level reached 4.0 metres above Australian height Datum (AHD) near Voaden Point (at the southern end of the Lockhart River Aboriginal Reserve). • Extensive environmental damage in vicinity of landfall location. • Cyclone recrossed Queensland west coast into Gulf of Carpentaria 70km south of Weipa. • Storm tide exceeded the Highest Astronomical Tide (HAT) at Cooktown by 0.28m. • National Disaster Relief Funding activated by Queensland Emergency Services Minister. Figure 1 –Track of severe tropical cyclone Ingrid (based on Tropical Cyclone Advices from Bureau of Meteorology). Summary Severe tropical cyclone Ingrid formed in the Coral Sea some time around 14:00 (AEST) on Sunday 6 March 2005 after drifting eastwards across Cape York along a monsoon trough line extending through northern Australia. The first Tropical Cyclone Advice was issued by the Bureau of Meteorology in Brisbane at 15:56 (AEST) on Monday 7 March, at which time Ingrid had deepened into a Category 3 cyclone (on a scale of 1 to 5). The timing of the cyclone corresponded to high spring tides, at or near the Highest Astronomical Tide (HAT), along the east coast of Cape York Peninsula, between Cairns and Thursday Island. Environmental Protection Agency (EPA) storm tide advisers reported to the Department of Emergency Services, State Disaster Coordination Centre at 13:00 (AEST) on Tuesday 8 March. -
Tropical Cyclone Risk and Impact Assessment Plan Final Feb2014.Pdf
© Commonwealth of Australia 2013 Published by the Great Barrier Reef Marine Park Authority Tropical Cyclone Risk and Impact Assessment Plan Second Edition ISSN 2200-2049 ISBN 978-1-922126-34-4 Second Edition (pdf) This work is copyright. Apart from any use as permitted under the Copyright Act 1968, no part may be reproduced by any process without the prior written permission of the Great Barrier Reef Marine Park Authority. Requests and enquiries concerning reproduction and rights should be addressed to: Director, Communications and Parliamentary 2-68 Flinders Street PO Box 1379 TOWNSVILLE QLD 4810 Australia Phone: (07) 4750 0700 Fax: (07) 4772 6093 [email protected] Comments and enquiries on this document are welcome and should be addressed to: Director, Ecosystem Conservation and Resilience [email protected] www.gbrmpa.gov.au ii Tropical Cyclone Risk and Impact Assessment Plan — GBRMPA Executive summary Waves generated by tropical cyclones can cause major physical damage to coral reef ecosystems. Tropical cyclones (cyclones) are natural meteorological events which cannot be prevented. However, the combination of their impacts and those of other stressors — such as poor water quality, crown-of-thorns starfish predation and warm ocean temperatures — can permanently damage reefs if recovery time is insufficient. In the short term, management response to a particular tropical cyclone may be warranted to promote recovery if critical resources are affected. Over the long term, using modelling and field surveys to assess the impacts of individual tropical cyclones as they occur will ensure that management of the Great Barrier Reef represents world best practice. This Tropical Cyclone Risk and Impact Assessment Plan was first developed by the Great Barrier Reef Marine Park Authority (GBRMPA) in April 2011 after tropical cyclone Yasi (one of the largest category 5 cyclones in Australia’s recorded history) crossed the Great Barrier Reef near Mission Beach in North Queensland. -
Storm Surge: Know Your Risk in Queensland!
Storm Surge: Know your risk in Queensland! Storm surge is a rise in sea level above the normal tide usually associated with a low pressure weather system such as a tropical cyclone. Storm surge develops due to strong winds pushing water towards the coastline as well as the low atmospheric pressure drawing up the sea surface. The Queensland coastline is highly vulnerable to storm surge. This is due to the frequency of tropical cyclones, the wide continental shelf and relatively shallow ocean floor in both the Great Barrier Reef lagoon and in the Gulf of Carpentaria, as well as the low lying nature of many coastal cities and towns. While the highest storm surges are more likely to occur in North Queensland and the Gulf of Carpentaria, they can also develop in southeast Queensland affecting the Sunshine Coast, Moreton Bay and the Gold Coast. Storm surges may reach magnitudes of 1 to 10 metres above the tide depending on the intensity of the cyclone, its size and the local characteristics of the coastline. Impacts Coral Sea Storm surge can be very dangerous and poses a critical risk Gulf of Carpentaria to human life during tropical cyclones. Great Cairns Barrier Reef The length of coastline affected by a storm surge can be Innisfail tens to hundreds of kilometres wide. The rise in sea level Cardwell Townsville can be rapid and high in velocity, inundating the ground Bowen floor of buildings, even up to the roof. Mackay Queensland Storm surge has the power to easily move cars, even Gladstone houses, can damage roads and buildings and can be Hervey Bay almost impossible to manoeuvre through. -
Identification of Climate Change Adaptation Best Practices in the Waste Management Sector ______
Identification of climate change adaptation Best Practices in the Waste Management Sector ___________________________________________ Disaster Waste Management Best practices FINAL REPORT – SEPTEMBER 4TH , 2013 IDENTIFICATION OF CLIMATE CHANGE ADAPTATION BEST PRACTICES IN THE WASTE MANAGEMENT SECTOR PART I REVISIONS VERSION DATE COMMENTS AUTHOR : CHECKED Final document incl. 2 02/09/2013 MLL ThM comments from client 1 19/08/2013 Final document MLL & JW ThM 0 09/08/2013 Draft document part I MLL & JW ThM This document is submitted by Pöyry France – Pöyry France becomes Naldeo Contact : Thierry Martin Manager International Department Naldeo France Phone + 33.4.91.13.97.56 Mobile + 33.6.82.56.92.94 55 rue de la Villette 69425 Lyon cedex 03 - France E-mail : [email protected] Page 2 NALDEO- PÖYRY 2013 IDENTIFICATION OF CLIMATE CHANGE ADAPTATION BEST PRACTICES IN THE WASTE MANAGEMENT SECTOR PART I CONTENTS PART I 1 IDENTIFICATION OF GEOGRAPHIC AREAS AFFECTED BY DESTRUCTIVE EVENTS LINKED TO CLIMATE CHANGE ................................................................................................................ 11 1.1 Effects of climat change .............................................................................................................. 11 1.1.1 Effects of climate change in the Pacific Region .....................................................................................................................11 1.1.2 Affected geographic areas ......................................................................................................................................................13 -
The Age Natural Disaster Posters
The Age Natural Disaster Posters Wild Weather Student Activities Wild Weather 1. Search for an image on the Internet showing damage caused by either cyclone Yasi or cyclone Tracy and insert it in your work. Using this image, complete the Thinking Routine: See—Think— Wonder using the table below. What do you see? What do you think about? What does it make you wonder? 2. World faces growing wild weather threat a. How many people have lost their lives from weather and climate-related events in the last 60 years? b. What is the NatCatService? c. What does the NatCatService show over the past 30 years? d. What is the IDMC? e. Create a line graph to show the number of people forced from their homes because of sudden, natural disasters. f. According to experts why are these disasters getting worse? g. As human impact on the environment grows, what effect will this have on the weather? h. Between 1991 and 2005 which regions of the world were most affected by natural disasters? i. Historically, what has been the worst of Australia’s natural disasters? 3. Go to http://en.wikipedia.org/wiki/File:Global_tropical_cyclone_tracks-edit2.jpg and copy the world map of tropical cyclones into your work. Use the PQE approach to describe the spatial distribution of world tropical cyclones. This is as follows: a. P – describe the general pattern shown on the map. b. Q – use appropriate examples and statistics to quantify the pattern. c. E – identifying any exceptions to the general pattern. 4. Some of the worst Question starts a. -
MASARYK UNIVERSITY BRNO Diploma Thesis
MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION DEPARTMENT OF ENGLISH LANGUAGE AND LITERATURE Presentation Sentences in Wikipedia: FSP Analysis Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský Declaration I declare that I have worked on this thesis independently, using only the primary and secondary sources listed in the bibliography. I agree with the placing of this thesis in the library of the Faculty of Education at the Masaryk University and with the access for academic purposes. Brno, 30th March 2018 …………………………………………. Bc. Lukáš Opavský Acknowledgements I would like to thank my supervisor, doc. Mgr. Martin Adam, Ph.D. for his kind help and constant guidance throughout my work. Bc. Lukáš Opavský OPAVSKÝ, Lukáš. Presentation Sentences in Wikipedia: FSP Analysis; Diploma Thesis. Brno: Masaryk University, Faculty of Education, English Language and Literature Department, 2018. XX p. Supervisor: doc. Mgr. Martin Adam, Ph.D. Annotation The purpose of this thesis is an analysis of a corpus comprising of opening sentences of articles collected from the online encyclopaedia Wikipedia. Four different quality categories from Wikipedia were chosen, from the total amount of eight, to ensure gathering of a representative sample, for each category there are fifty sentences, the total amount of the sentences altogether is, therefore, two hundred. The sentences will be analysed according to the Firabsian theory of functional sentence perspective in order to discriminate differences both between the quality categories and also within the categories. -
Seasonal Climate Summary for the Southern Hemisphere (Autumn 2018): a Weak La Nin˜A Fades, the Austral Autumn Remains Warmer and Drier
CSIRO PUBLISHING Journal of Southern Hemisphere Earth Systems Science, 2020, 70, 328–352 Seasonal Climate Summary https://doi.org/10.1071/ES19039 Seasonal climate summary for the southern hemisphere (autumn 2018): a weak La Nin˜a fades, the austral autumn remains warmer and drier Bernard ChapmanA,B and Katie RosemondA,B ABureau of Meteorology, GPO Box 413, Brisbane, Qld 4001, Australia. BCorresponding authors. Email: [email protected]; [email protected] Abstract. This is a summary of the austral autumn 2018 atmospheric circulation patterns and meteorological indices for the southern hemisphere, including an exploration of the season’s rainfall and temperature for the Australian region. The weak La Nin˜a event during summer 2017–18 was in retreat as the southern hemisphere welcomed the austral autumn, and before midseason, it had faded. With the El Nin˜o Southern Oscillation and the Indian Ocean Dipole in neutral phases, their influence on the climate was weakened. Warmer than average sea surface temperatures dominated much of the subtropical South Pacific Ocean and provided favourable conditions for the formation of a rare subtropical cyclone over the southeast Pacific Ocean in May. The southern hemisphere sea ice extent was slightly below the autumn seasonal average. The southern hemisphere overall during autumn was drier and warmer than the seasonal average. The season brought warmer than average temperatures and average rains to parts of the continents of Africa and South America. Australia recorded its fourth-warmest autumn, partly due to an intense, extensive and persistent heatwave, which occurred during the midseason. An extraordinary and record-breaking rainfall event occurred over Tasmania’s southeast, under the influence of a negative Southern Annular Mode.